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The vertical structure of temperature and humidity fields in the atmospheric boundary layer over Western Siberia in clear air and in the presence of continuous cloudiness

Abstract

The peculiarities of the vertical structures of temperature and water vapor mass fraction fields in the atmospheric boundary layer of Western Siberia typical for clear air and continuous cloudiness of the lower layer are discussed.

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References

  1. 1.

    K. Ya. Kondrat’ev and Yu. M. Timofeev, Meteorological Sensing of the Atmosphere from Space (Gidrometeoizdat, Leningrad, 1978) [in Russian].

    Google Scholar 

  2. 2.

    V. E. Zuev and V. V. Zuev, Remote Optical Sensing of the Atmosphere (Gidrometeoizdat, St. Petersburg, 1992) [in Russian].

    Google Scholar 

  3. 3.

    V. S. Komarov and N. Ya. Lomakina, Statistical Models of Atmosphere Boundary Layer of Western Siberia (IOA SO RAN, Tomsk, 2008) [in Russian].

    Google Scholar 

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Correspondence to V. S. Komarov.

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Original Russian Text © V.S. Komarov, N.Ya. Lomakina, S.N. Il’in, 2010, published in Optica Atmosfery i Okeana.

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Komarov, V.S., Lomakina, N.Y. & Il’in, S.N. The vertical structure of temperature and humidity fields in the atmospheric boundary layer over Western Siberia in clear air and in the presence of continuous cloudiness. Atmos Ocean Opt 23, 28–31 (2010). https://doi.org/10.1134/S1024856010010069

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Keywords

  • Atmospheric Boundary Layer
  • Vertical Structure
  • Oceanic Optic
  • Cloud Amount
  • Humidity Field